Optical and Physical Properties of the Carbon Tetrachloride Solvate of

to determine its principal optical and physical properties. The material used for the study was a sample of rotenone that had been recrystallized seve...
0 downloads 0 Views 873KB Size
'May, 1937

THR

CARBON

TETRACIIWRIDE SOLVATE OF

nf trimethylamine upon cithcr bnrine carbonyl or diborane. The behavior of ammonia toward diborane and toward borine carbonyl is quite dif-

ROTENONE

787

fercnt from that of trimethylamine toward thew reagents. CHIWOO. II,~.INOIR RRCRNED F E B R U in. ~ Y1837

(CONTRlBvtlON FROM THE BUREAU OF ENTOHOLoCY AND m A N T

QUARANTINE, U. S. DEPARTMENT OF AORICULTURR]

Principal Optical and Physical Properties of the Carbon Tetrachloride Solvate of Rotenone BY ERNEST L. GOODENAND CHARLES M. SMITH

For several years chemists and manufacturers working with rotenone have been familiar with the carbon tetrachloride solvate, in which one molecule of rotenone is combined with one molecule of carbon tetrachloride of crystallization (GHaO&ClJ.' Since this solvate is of great practical importance, especially in the analysis of derris and cuM, it was considered necessary to determine its principal optical and physical properties. The material used for the study was a sample of rotenone that had been recrystallized several times and subjected to microdetermination of carbon and hydrogen to gain assurance of purity.' A portion of this analyzed sample was recrystallized from carbon tetrachloride to form the carbon tetrachloride solvate.

-

Optical Crystallographic Properties The optical properties investigated were such

as are determinable by the use of the petrographic microscope. The solvate crystals were colorless. with a typical elongated, somewhat flattened prismatic shape (Fig. 1). The crystals were found to be biaxial with the following refractive indices (white light): u = I.563, 9 , = 1.612, y = 1.631. The indication of negative optical character obtained by the selenite plate is fairly distinct, and the observed value of @ is so much nearer y than u as to allow no doubt that the character is truly negative. In all cases observed the elongation is negative, the long edges of the crystal lying in the vibration direction for u. Extinction is sensibly parallel at all stages of rotation about the axis of crystal length, which is the vibration direction for u. It is concluded that the crystal belonp in the orthorhombic system.

-

ERNEST L. GOODEN AND CHARLES M. SMITH

788

The temperature readings were corrected by the established correction curve for the individual thermometer, and the manometer readings were corrected for temperaure of the mercury. With each bath liquid the rise in pressure in the space above the sample was observed repeatedly arid the gas was released (for the elimination of air) between successive sets of observations, until a sufficiently precise determination of limiting pressure for given temperature was obtained. Two observed values of limiting pressure were obtained with each of the three baths, giving six points for determination of the vapor pressure curve. When these points were plotted as log pressure (in millimeters of mercury) against 50 2.9

Temperature in “ C . 70 90 I I

- 700 - 600 - 500 - 400 li

E -300

2P

2 - 200

- 150 0.0029 0.0027 1/abs. temp. Fig. Z.-Dissocistion pressure of the carbon tetrachloride solvate of rotenone (pressure of CC14 vapor over ChHaOo CHH~ZOCCCL). 0.0031

+

VOl. 59

and is expressed by the equation log P = 9.308 - (2313/T) where P is the pressure in millimeters of mercury and T i s the temperature on the absolute (Kelvin) scale. The six points and the calculated line are shown in Fig. 2. This equation leads to a value of S T O for what may be termed the “decomposition temperature’’ of the solvate, in the sense of the temperature a t which the carbon tetrachloride vapor reaches normal atmospheric pressure. The heat of dissociation-vaporization as calculated on the basis of the same equation is 69 cal. per gram of carbon tetrachloride, which is approximately 23 cal. per gram in excess of the heat of vaporization of carbon tetrachloride at the same temperature. These results indicate that the solvate is so unstable as to require careful sealing for storage. Additional Comparisons and Checks It is interesting and worth while to compare the optical properties of the carbon tetrachloride solvate of rotenone with those of rotenone itself in the common (m. p. 163’) form. The indices ,9 and y of the solvate nearly coincide, respectively, with a and ,9 of rotenone (a = 1.616, ,9 = 1.635, y = 1.662); the maximum birefringence, however, is one and one-half times as great in the solvate as in rotenone. The specific refraction is conspicuously lower in the solvate, as would be expected from the fact that the specific refraction of carbon tetrachloride is approximately 36% lower than that of rotenone. The calculated molecular refraction cannot be arrived a t precisely because of the complex structure of rotenone. The various calculated values for the molecular refraction of the solvate are all very close to 129 (cubic centimeters per mole, according to Lorentz-Lorenz formula), if no allowance is made for a linkage refraction for the combination of the rotenone molecule with the carbon tetrachloride molecule. The observed molecular refraction is 134, this value being nearly equal to the sum of the observed molecular refraction (107) for rotenone and the observed value (26.45) for carbon tetrachloride.

reciprocal of absolute temperature, they were summary found to lie almost exactly in a straight line. The best fitting straight line was ~alculated,~ The carbon tetrachloride solvate of rotenone, CzaH~O.yCCl~, has been studied with respect to (4) One of the six points, the lowest, showed an appreciable departure from a straight line, and was therefore disregarded; the line refractive indices, density and dissociation preswas calculated from the other five points by the method of least sure * squares.

THECRYSTAL STRUCTURE OF SELENIUM DIOXIDE

May, 1937

The principal results of the optkal determinatioiis are: (Y = 1.563; p = 1.612; y = 1.631; optical character] negative; elongation, commonly negative; system, orthorhombic. The density at 30' is 1.40 g. per cc. T h e dissociation pressrire in the range (io to

789

is expressed by the equatioll log Pmm,= 9.308 ('2313/T~). The "decomposition temperature" is consequently 8To, and the heat of dissociation-vaporization 69 calories per gram ()f carbon tetrachloride. \\'ASHIN(;[()N, 1) c RFCEIVEDFRRRTJARY 17, 1937

90'

-

THE GATESCHEMICAL LABORATORY, CALIFORNIA INSTITUTEOF TECHNOLOGY, CHEMICAL LABORATORY OF THE UNIVERSITY OF CALIFORNIA AT L O S ANGELES]

[CONTRIBUTION FROM

No. 584, AND THE

The Crystal Structure of Selenium Dioxide BY JAMES D. MCCULLOUGH Quoting measurements made by C. F. Rammels- tablished by noting that a rotation of 90' about burg, Groth' describes selenium dioxide as mono- the needle axis gave a Laue photograph indisclinic prisms with n : b : c = 1.2@2:1:1.067. He tinguishable from the original one. Further states that the measurements were only approxi- evidence was furnished by the fact that the mate, however, due to the extreme hygroscopic photographs prepared with the x-ray beam nature of the crystals, which made rapid work parallel to the needle axis showed a fourfold necessary. All crystals examined in the present axis and four planes of symmetry at 45' intervals. work were found to be tetragonal needles with The Laue symmetry thus indicated is that of the axial ratio. a : c = 1:0.6047. Dlh. A complete set of 15' oscillation photographs Method of Preparation.-Pure selenium dioxide was dried at approximately 200' in a stream was prepared using unfiltered copper radiation of oxygen which had been passed first through a with a 5-cm. camera. The oscillation was about tube containing phosphorus pentoxide. After the c-axis. One 30' oscillation photograph was drying for several hours, the Pyrex tube coii- prepared using [110] as an axis but was not very taining the selenium dioxide was sealed of? at satisfactory for intensity considerations due to both ends and the substance was sublimed the shape of the crystal. Attempts to cleave very slowly in an electric furnace. The atmos- the crystals across the needle or c-axis were phere of oxygen prevented the decomposition unsuccessful and resulted in shattering. which sometimes accompanies sublimation of From these photographs the unit edges a. the oxide in the open. The tube was opened = 8.353 * 0.005 8.and co = 5.051 * 0.010 A. inside a moisture-free box and selected crystals were calculated. Using these dimensions, values were mounted in moisture-proofed gelatine cap- of nX were calculated for a completely indexed sules. Except when being photographed they Laue photograph in which the x-ray beam made were kept in a desiccator. These precautions an angle of about 2' with the a-axis. The smallwere found necessary in order to preserve the est value thus found was nh = 0.245 8. from crystal faces and prevent lines due to selenious (810), the short wave length limit being 0.24 8. acid appearing on the photographs. The oscillation photographs and the first order The crystals were transparent, colorless needles reflections on the indexed Laue photograph about 2-10 mm. long and 0.2-0.5 mm. thick with showed all varieties of (hkl) and (hkO) reflections. (loo), (110) and (1 11) principally developed. The lattice is accordingly simple. Reflections of the type (hhl) were not observed for I odd The Unit Cell and Space-Group although many such planes were in position to Laue photographs prepared with the incident reflect,- especially on the oscillation photograph beam perpendicular to a (100) face showed a about [llO]. Further, (h01) was not observed vertical as well as a horizontal plane of symmetry for h odd. These conditions indicate Diias did the photographs normal to a (110) face. P4/mbc or C:v - C4cb as probable space groups. The tetragonal nature of the crystals was es- Attempts to detect a pyroelectric effect failed, (1) P. Groth. "Chemische Kristallographie." yoi I, 1 ~ 0 6p. , 93. but this may have been due to the hygroscopic